page Taranaki Regional Council Monthly Rainfall and Environmental Data Report for August 2022 02 September, 2022 Provisional Data Only. Note: some sites record a number of parameters 1. Rain gauge values throughout the region Note: Taranaki co-owns rain-gauges with Horizons, so we can assess rainfalls right-out over the Eastern Hill Country. Map1: Rain gauge sites page Table 1: Rainfall monthly and year to date totals at 27 rain gauge sites in
https://www.nems.org.nz/documents/water-quality-part-3-lakes/ page Technical Memorandum | Draft Baseline State for Escherichia coli and Cyanobacteria (Planktonic) in Taranaki Rivers and Lakes year at 40 popular primary contact sites, including a range of beaches, rivers and lakes around Taranaki. There are 23 freshwater sites (i.e. rivers and lakes) included in the current CISH programme. The monitoring results highlight the impact that rainfall has on recreational water quality. Escherichia coli concentrations can be
page Map1: Rain gauge sites Table 1: Rainfall monthly and year to date totals at 27 rain gauge sites in Taranaki. June Year to Date Hydro_Sites # days > 0.5 mm Total Rainfall (mm) % of typical month Total to date (mm) % of typical year to date % of typical full year Records Began North Egmont at Visitors Centre 8 658.0 98.4 2915.0 99.0 43.4 1991 Dawson Falls 5 906.0 191.2 3102.5 151.4 68.9 1933 Kahui
during the 2021-2022 monitoring year, with south Taranaki commencing irrigation in November and the rest of the region beginning in January. Irrigation concluded late April through to early May across the region. Rainfall recorded at the Council’s monitoring locations over the summer irrigation period ranged between 82% and 203% of historical mean values. Even though rainfall volumes were higher than previous years, the irrigation season was longer with total irrigation water usage of 6,960 ML
forming a tributary of the much larger Mimitangiatua awa catchment. It runs from south-east to north-west. Almost the entire valley formed by the Stream is owned by the Company, and consists of steep eroded hillsides, multiple side gullies, and small river flats distributed along its length. The area receives more rainfall than the northern Taranaki coastline to the south-west. Soils are generally poor and highly erodible. Patches of bush and planted trees cover most of the hillsides, with the
a week between 1 November and 31 March each year at 40 popular primary contact sites, including a range of beaches, rivers and lakes around Taranaki. There are 23 freshwater sites (i.e. rivers and lakes) included in the current CISH programme. The monitoring results highlight the impact that rainfall has on recreational water quality. Escherichia coli concentrations can be significantly elevated at primary contact sites for up to three days following heavy rainfall. This is owing to the
page Monthly Year to Date Hydro_Sites # days > 0.5 mm Total Rainfall (mm) % of typical month Total to date (mm) % of typical year to date % of typical full year Records Began North Egmont at Visitors Centre 17 713.0 112.0 2257.0 99.2 33.6 1991 Dawson Falls 16 555.0 120.1 2196.5 139.5 48.8 1933 Kahui Hut 20 563.5 125.2 1665.0 101.3 34.5 2006 Mangorei Upper at Forest Hill 17 450.5 118.6 1512.0
d) Construction timetable for the erosion and sediment control works and the bulk earthworks proposed; e) Maintenance, monitoring and reporting procedures; f) Rainfall response and contingency measures including procedures to minimise adverse effects in the event of extreme rainfall events and/or the failure of any key erosion and sediment control structures; g) Procedures and timing for review and/or amendment to the erosion and sediment control measures listed in the ESCP; and,
Manawa Energy Patea HEP Annual Report 2022-2023
also be a potential indicator of intensive land use impact where fertiliser is applied to land (Rosen, 2001). - - - - - - Chloride (Cl) Chloride is relatively unaffected by geochemical processes which makes it a good indicator of general groundwater quality. The primary source of chloride in groundwater is marine sourced rainfall recharge to an aquifer. However, saltwater intrusion and land use activities, such as wastewater and effluent discharges, can contribute chloride to …